TY - RPRT
T1 - Meteorological Uncertainty of atmospheric Dispersion model results (MUD)
T2 - Final Report of the NKS-B MUD activity
AU - Havskov Sørensen, Jens
AU - Amstrup, Bjarne
AU - Feddersen, Henrik
AU - Smith Korsholm, Ulrik
AU - Bartnicki, Jerzy
AU - Klein, Heiko
AU - Wind, Peter
AU - Lauritzen, Bent
AU - Cordt Hoe, Steen
AU - Israelson, Carsten
AU - Lindgren, Jonas
PY - 2014
Y1 - 2014
N2 - The MUD project addresses assessment of uncertainties of atmospheric dispersion model predictions, as well as optimum presentation to decision makers. Previously, it has not been possible to estimate such uncertainties quantitatively, but merely to calculate the 'most likely' dispersion scenario. However, recent developments in numerical weather prediction (NWP) include probabilistic forecasting techniques, which can be utilised also for atmospheric dispersion models.
The ensemble statistical methods developed and applied to NWP models aim at describing the inherent uncertainties of the meteorological model results. These uncertainties stem from e.g. limits in meteorological obser-vations used to initialise meteorological forecast series. By perturbing the initial state of an NWP model run in agreement with the available observa-tional data, an ensemble of meteorological forecasts is produced. In MUD, corresponding ensembles of atmospheric dispersion are computed from which uncertainties of predicted radionuclide concentration and deposition patterns are derived.
AB - The MUD project addresses assessment of uncertainties of atmospheric dispersion model predictions, as well as optimum presentation to decision makers. Previously, it has not been possible to estimate such uncertainties quantitatively, but merely to calculate the 'most likely' dispersion scenario. However, recent developments in numerical weather prediction (NWP) include probabilistic forecasting techniques, which can be utilised also for atmospheric dispersion models.
The ensemble statistical methods developed and applied to NWP models aim at describing the inherent uncertainties of the meteorological model results. These uncertainties stem from e.g. limits in meteorological obser-vations used to initialise meteorological forecast series. By perturbing the initial state of an NWP model run in agreement with the available observa-tional data, an ensemble of meteorological forecasts is produced. In MUD, corresponding ensembles of atmospheric dispersion are computed from which uncertainties of predicted radionuclide concentration and deposition patterns are derived.
KW - NKS-307
KW - Nuclear emergency preparedness
KW - Atmospheric dispersion model
KW - Meteorology
KW - Uncertainty
KW - Ensemble prediction
M3 - Report
T3 - NKS
BT - Meteorological Uncertainty of atmospheric Dispersion model results (MUD)
PB - NKS Secretariat
ER -